Flammeovirga sp. SJP92琼脂酶的分离纯化及其酶学性质

琼胶酶是一类能够降解琼脂糖生成琼胶寡糖的酶类,具有广泛的应用范围.从海洋性高产琼胶酶菌株Flammeovirga sp. SJP92的发酵液经硫酸铵沉淀,DEAE 琼脂糖离子层析,分离纯化获得了一个分子量约为70KDa的琼胶酶AgaB.经过酶学性质分析,它的最适pH值为70,最适温度为40℃,在最适温度下能够保持较好的稳定性.进一步的分析表明, MgSO4和β Me对该酶有明显的促进作用,而CaCl2、MnCl2、ZnCl2、CoCl2、FeCl3、CuSO4等则会强烈抑制它的活性.此外,通过产物分析表明,该酶能够通过内切作用将琼脂糖最终降解成6糖和4糖.AgaB的分离纯化及其酶学性质分析为其工业应用奠定了基础.     

一株卓贝尔氏菌F13-1好氧反硝化特性及其反硝化基因的初步研究

为获得高效好氧反硝化细菌,并研究这些细菌的脱氮特性以及好氧反硝化机理,采集了近海表层沉积物进行富集培养,分离获得一株具有高效好氧反硝化能力的菌株F13-1.结合生理生化特征及16S rRNA基因序列分析,初步鉴定菌株F13-1为卓贝尔氏菌(Zobellella sp.).在以葡萄糖为碳源,C/N比值为15,盐度为30,摇床转速160 r/min,p H值为7,28℃的最优脱氮条件下菌株F13-1脱氮效果较好,分别能将100 mg/dm3硝酸盐和亚硝酸盐在24和16 h内彻底脱除,脱除速率分别为:5.87 mg/(dm3·h)和5.97 mg/(dm3·h).并且菌株F13-1对高浓度亚硝酸盐具有较好的耐受性,能在高浓度亚硝酸盐存在条件下正常生长及脱氮,156 h内能将400 mg/dm3亚硝酸盐脱除完全.基因组分析表明,该菌株具有完整的反硝化基因簇,包括nap、nir、nor和nos等共17个基因.研究结果表明该菌株具有高效好氧反硝化特性,在养殖废水处理中具有较好的应用潜力.     

高压旋喷法在漂卵石冲洪积土软基处理中的应用

对于厚层的含漂卵石的山前冲洪积土软弱地基,采用常规的CFG桩、水泥搅拌桩进行地基处理,存在成孔难,复合地基承载力偏低等问题。本文以桂平市某高层商住楼工程为例,介绍了高压旋喷桩复合地基的设计和加固效果检测,结果表明,采用潜孔钻机引孔+高压旋喷桩加固技术处理含漂卵石软弱地基,能有效地解决成孔难问题,也大大提高了地基承载力和成桩效率。     

First record of Ostreopsis cfr. ovata on macroalgae in the Northern Adriatic Sea

Ostreopsis ovata is an epiphytic potentially toxic dinoflagellate. It has a world-wide distribution, normally associated with other epiphytic or benthic dinoflagellates. In tropical seas O. ovata is often associated with the genera Gambierdiscus, Coolia and Prorocentrum, causing cinguatera fish poisoning. Recently, Ostreopsis spp. blooms in the Tyrrhenian and southern Adriatic Sea have been related to human health problems, such as breathing and skin irritation. Here we report the first record of Ostreopsis cfr. ovata in the Northern Adriatic Sea. O. cfr. ovata was isolated from macroalgae in two areas, the Gulf of Trieste (Italy) and close to Rovinj (Croatia). The microalga was identified by scanning electron microscopy and by fluorescence light microscopy. Size range and thecal pore structure were similar to those described for O. cfr. ovata in previous studies. Ostreopsis cfr. ovata was present on all the macroalgae collected, particularly browns and reds. The microalgal association on macroalgae was mostly composed of Ostreopsis sp., Coolia monotis and Coscinodiscus sp.     

中国南海软珊瑚附生真菌Acremonium sp. SCSIO41216的次级代谢产物研究

采用硅胶柱层析色谱法、中压正相柱层析色谱法、中压反相柱层析色谱法以及半制备高效液相色谱法对中国南海软珊瑚来源真菌Acremonium sp. SCSIO41216的大米发酵产物进行分离纯化, 并使用核磁共振、质谱等波谱学方法, 结合其理化性质及文献数据鉴定了7个单体化合物结构: fischexanthone(1)、sydowinin A (2)、(22E)-5α,8α-epidioxyergosta-6,22-dien-3β-ol (3)、16-O-去乙酰基夫西地酸内酯(4)、环-(S)-脯氨酸-(R)-亮氨酸(5)、环-(S)-脯氨酸-8-羟基-(R)-异亮氨酸(6)和环(L)-脯氨酸-(L)-苯丙氨酸(7)。化合物1—7均首次从海洋软珊瑚来源的枝顶孢属真菌(Acremonium sp.)中分离获得。     

A pore-throat model based on grain-size distribution to quantify gravity-dominated DNAPL instabilities in a water-saturated homogeneous porous medium

A pore-scale network model based on spherical pore bodies and cylindrical pore throats was developed to describe the displacement of water by DNAPL. The pore body size and the pore throat size were given by statistical distributions with user-specified values for the minimum, mean and maximum sizes. The numerical model was applied to a laboratory experiment conducted on a sand-filled glass column. The parameters relative to pore body size and pore throat size that were used in the construction of the equivalent network were derived from the discrete grain-size distribution of the real porous medium. The calculated arrival times of the DNAPL front were compared with those measured using optic fibre sensors placed at different points on the control section of the experimental device. Furthermore, the model simulated DNAPL pressure measured at the entrance section of the system. In general, the numerical results obtained with the model were in good agreement with the actual measurements.     

红鳍东方鲀(Takifugu rubripes)形态性状对体重的影响效果

采用通径分析方法,对红鳍东方鲀表型形态性状对体重的影响效果进行研究.结果表明,所测各表型性状与体重之间的相关系数均达到显著水平(P＜0.05)或极显著水平(P＜0.01);体周长1对体重的直接影响(0.533)最大,对体重的决定程度(28.41％)最高,是影响体重的主要因素;全长对体重的直接作用(0.369)较大,间接作用(0.259)最小;体高、尾柄高对体重的直接作用(0.228,0.145)相对较小,主要通过体周长1的间接作用(0.363,0.296)影响体重.所选表型性状对体重的复相关指数R2=0.950,表明所选性状是影响体重的主要性状.利用逐步回归分析方法建立以体周长1、体高、尾柄高为自变量估计体重的多元回归回归方程为:y =-2154.095+42.072x1+33.936x2+72.687x3+50.538x4.     

Late-time photometry of two nearby type Ⅱ-P supernovae: 2004dj and 2004et

We present late-time photometry for two bright type Ⅱ-P supernovae (SNe) 2004dj and 2004et, extending over 400 d after the explosion, which are measured with a set of intermediate-band filters that have the advantage of tracing the strength variations of some spectral features. Although these two SNe Ⅱ-P exhibit similar photometric evolution at earlier times, they diverge during the nebular phase. SN 2004dj shows a slow late-time decline rate with ～0.7±0.1 mag (100d)-1 during the period ranging from t≈200-300 d after the explosion, while SN 2004et shows a much faster decline rate at a comparable phase, e.g., 1.3±0.1 mag (100d)-1. The steeper decay rate seen in SN 2004et is likely due to dust formation in the explosion ejecta. Based on intermediate-band photometry, we derived the evolution of the feature lines [e.g., Hα] of SNe 2004dj and 2004et which are similar in flux at comparable phases but perhaps with significantly different decay rates. The origin of the observed variations in the continuum and the feature lines is briefly discussed.     

建鲤与黄河鲤的RAPD分子标记及其杂交优势的遗传分析

利用RAPD技术对建鲤、黄河鲤及其杂交子代进行了遗传分析,筛选的33个引物共扩增出155条带,其中多态性片段为105条,片段S18-1600、S472-300具有种的特异性,可作为鉴别建鲤与黄河鲤的分子遗传标记。建鲤、黄河鲤及其正、反交子代群体内的遗传相似系数分别为0.8240、0.7921、0.7920、0.8569,黄河鲤与正交F1具有较高的遗传变异水平,反交F1变异最小。正交F1、反交F1与亲本(建鲤、黄河鲤)的遗传距离分别为0.2233、0.2436、0.1749、0.2026,说明子代均继承了较多的建鲤的遗传物质。分析了子代与亲本的RAPD标记类型以及各类型的条带数。应用PIT标记系统测定了子代的杂种优势并探讨了优势产生的遗传机理。     

Mn-oxide: a major source of easily mobilisable Co and Ni under reducing conditions in New Caledonia FerralsolsLes oxydes de Mn : une source majeure de Co et Ni facilement mobilisables en conditions réductrices dans les Ferralsols de Nouvelle-Calédonie

Chemical and bacterial reduction and dissolution of Fe and Mn-oxide and the concomitant solubilisation of Co and Ni were studied in a surface horizon of a New-Caledonia Ferralsol. Chemical extractions showed that Mn and Co were in a large part associated in Mn-oxides. The main part of Ni was associated with goethite, but a very small fraction was also associated with Mn-oxides. Anaerobic reducing bacterial activity was responsible for Fe solubilisation at a smaller extent than for Mn solubilisation and consequently for associated metal release. Submicroscopic investigations revealed the presence of a Mn-oxide containing Co, Ni and Al, close to a lithiophorite–asbolane mixed-layers Mn-oxide, which can be considered as a main source of easily available metals in this soil. To cite this article: C. Quantin et al., C. R. Geoscience 334 (2002) 273–278.